在一个活跃的火山中将石化学和地震学联系起来
Kate Saunders1, Jon Blundy, Ralf Dohmen
1Department of Earth Sciences, University of Bristol, Bristol, UK. Kate.Saunders@bristol.ac.uk
概括
火山动荡信号,就像地震一样,可以表明岩的运动. 研究来自圣海伦斯山的正氧化晶体揭示了岩入侵与地震事件相关,改善了喷发预测.
科学领域:
- * * 火山学 关于火山的研究
- * 石化学 石化学
- * * 地质物理学
背景情况:
- * 活火山在爆发前会发生地震性,地面变形和气体排放的变化.
- *将这些动荡信号解释为地下岩过程仍然是火山监测的一个重大挑战.
- *了解岩运动对于预测火山爆发至关重要.
研究的目的:
- * 调查岩入侵和火山爆发前的地震性之间的关系.
- *利用火山水晶的岩石学数据来了解地下的岩过程.
- *通过对喷发产物的详细分析,提高火山爆发预测的准确性.
主要方法:
- *分析了来自1980-1986年圣海伦斯山爆发的300多个带区的正氧化物晶体.
- *将扩散计时法应用于正氧化晶圈,以确定事件的时间.
- * 石油学数据与历史地震性记录的相关性.
主要成果:
- * ортопироксен晶体记录了新的岩和挥发性物质的脉冲入侵到一个更大的岩储库中.
- *扩散计时显示了岩入侵事件和记录的地震性之间的时间相关性.
- * 有证据表明,一些地震事件与岩入侵过程有直接联系.
结论:
- *对水晶的岩石学分析提供了关于爆发前岩活动的时间和性质的见解.
- * 岩入侵事件的时间尺度与在动荡的火山中观察到的监测信号一致.
- *这项研究通过将岩石学观测与地震监测数据联系起来,提高了预测火山爆发的能力.
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